The accumulation of detailed ion flux measurements from long-lived spacecraft orbiting the solar system's terrestrial planets have enabled recent studies to estimate the rate of solar …
E Dubinin, M Fraenz, A Fedorov, R Lundin… - The plasma environment …, 2012 - Springer
Mars and Venus do not have a global magnetic field and as a result solar wind interacts directly with their ionospheres and upper atmospheres. Neutral atoms ionized by solar UV …
We revisit the idea of 'terraforming'Mars—changing its environment to be more Earth-like in a way that would allow terrestrial life (possibly including humans) to survive without the need …
More than 7 years of ion flux measurements in the energy range 10 eV–15 keV have allowed the ASPERA‐3/IMA (Analyzer of Space Plasmas and Energetic Ions/Ion Mass …
We have used more than 4years of Mars Express ion data to estimate the escape of heavy ions (O+, O2+ and CO2+) from Mars. To take the limited field of view of the instrument into …
Abstract We study the Mars Atmosphere and Volatile Evolution spacecraft observations of Martian planetary ion escape during two time periods: 11 November 2014 to 19 March 2015 …
The magnetized solar wind drives a current system around Mars that maintains its induced magnetosphere. The solar wind also transfers its energy to the atmospheric ions, causing …
E Dubinin, M Fraenz, M Pätzold… - Journal of …, 2017 - Wiley Online Library
We present multi‐instrument observations of the effects of solar wind on ion escape fluxes on Mars based on the Mars Atmosphere and Volatile EvolutioN (MAVEN) data from 1 …
It is not yet entirely clear whether Mars began as a warm and wet planet that evolved towards the present-day cold and dry body or if it always was cold and dry with just some …